a) On the eastern slope, the height of the volcano changes by about 1500 meters over a distance of 4km. The gradient is therefore 1500/4 m/km = 375 m/km or 1980 ft/mile.
b) Based on the light grey color of the volcano in the Google Earth image and the slope in the DEM, the volcano is likely rhyolitic to andesitic in composition. i.e. acidic to intermediate.
c) Jamacas is located around 10 km from the volcano and has the greatest hazard potential in case of an eruption. Since the volcano is acidic to intermediate in composition, the greatest threat is posed by a pyroclastics that are spewed out during eruption rather than the flow itself, which would be too viscous to travel far. Evacuations would need to be conducted for a shorter radius than would be required if the flow were basic.
Exercise 2 In this exercise, students will evaluate the volcano Popocatépetl in Mexico 1. Using t...
Exercise : Volcano Shape The purpose of this exercise is to compare the slope of two volcanoes, Hawaii and Mt. St. Helens Hawai: The Hawaiian volcanoes are shield volcanoes, though some cinder cones are present as well. The very low viscosity of mafic/basaltic magma that cools to form the Hawaiian shield volcanoes produces very gentle or shallow slopes. This is a primary characteristic of shield volcanoes. So, let's try to get an impression of just how low the slopes of...